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首页> 外文期刊>Bulletin of the Seismological Society of America >Conditional Ground-Motion Model for Damaging Characteristics of Near-Fault Ground Motions Based on Instantaneous Power
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Conditional Ground-Motion Model for Damaging Characteristics of Near-Fault Ground Motions Based on Instantaneous Power

机译:基于瞬时动力的近端故障地面运动损伤特性条件地运动模型

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摘要

The velocity pulse in near-fault ground motions has been used as a key characteristic of damaging ground motions. Characterization of the velocity pulse involves three parameters: presence of the pulse, period of the pulse, and amplitude of the pulse. The basic concept behind the velocity pulse is that a large amount of seismic energy is packed into a short time, leading to larger demands on the structure. An intensity measure for near-fault ground motions, which is a direct measure of the amount of energy arriving in short time, called instantaneous power (IP (T-1)), is defined as the maximum power of the bandpassfiltered velocity time series measured over a time interval of 0.5 T-1, in which T-1 is the fundamental period of the structure. The records are bandpass filtered in the period band (0.2 T-1-3 T-1) to remove the frequencies that are not expected to excite the structure. Zerin and Abrahamson (2020) showed that the drift is better correlated with the IP (T-1) than with the velocity pulse parameters for records scaled to the same spectral acceleration at T-1. A conditional ground-motion model (GMM) for the root IP is developed based on the 5%-damped spectral acceleration at T-1, the earthquake magnitude, and the rupture distance. This conditional GMM can be used for record selection for near-fault ground motions that captures the key features of velocity pulses and can lead to a better representation of the median and variability of the maximum interstory drift. The conditional GMM can also be used in a vector hazard analysis for spectral acceleration (T-1) and IP (T-1) that can be used for more accurate estimation of drift hazard and seismic risk.
机译:近断层地震动中的速度脉冲已被用作破坏性地震动的关键特征。速度脉冲的表征涉及三个参数:脉冲的存在、脉冲的周期和脉冲的振幅。速度脉冲背后的基本概念是,大量地震能量被压缩到短时间内,从而对结构产生更大的要求。近断层地面运动的强度度量是对短时间内到达的能量量的直接度量,称为瞬时功率(IP(T-1)),定义为在0.5 T-1的时间间隔内测量的带通滤波速度时间序列的最大功率,其中T-1是结构的基本周期。在周期带(0.2 T-1-3 T-1)中对记录进行带通滤波,以去除预计不会激励结构的频率。Zerin和Abrahamson(2020)表明,漂移与IP(T-1)的相关性好于与T-1相同谱加速度下记录的速度脉冲参数的相关性。基于T-1处5%阻尼谱加速度、地震震级和破裂距离,建立了根IP的条件地震动模型(GMM)。该条件GMM可用于近断层地面运动的记录选择,该记录可捕捉速度脉冲的关键特征,并能更好地表示最大层间漂移的中值和可变性。条件GMM还可用于谱加速度(T-1)和IP(T-1)的矢量危险分析,可用于更准确地估计漂移危险和地震风险。

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